Carbonate grain types and assemblages
{"Image DocumentName": "Carbonate grain types and assemblages", "Image ImageDescription": "The skeletal grain associations that occur on carbonate platforms are temperature / suhu and salinity / kemasinan dependent. In low latitudes where the shallow sea is always over 15\u00b0C and the salinity is normal, corals and calcareous green algae are common and along with numerous other organisms form a chlorozoan assemblage. In restricted seas where the salinities are higher only green algae flourish, and form a chloralgal association. Temperate carbonates formed in cooler waters are dominated by the remains of benthic foraminifers and molluscs, a foramol assemblage. Ooids are most commonly associated with chlorozoan and chloralgal assemblages.", "Image XResolution": "37", "Image YResolution": "37", "Image ResolutionUnit": "Pixels/Centimeter", "Image Software": "SlidePlayer", "Image YCbCrPositioning": "Centered"}